CI[)l1:721 - Memorial University of Newfoundland DAI
CI[)l1:721 - Memorial University of Newfoundland DAI
CI[)l1:721 - Memorial University of Newfoundland DAI
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79<br />
Only two examples are known from Maine. One. in the Chandler canactian,<br />
cuated by the <strong>University</strong> <strong>of</strong> Maine at Orono, was collected from the 51. Croix<br />
River drainage (D. Sanger 1988: personal communication). The second is from<br />
Big lake. Washington County (5. Cox 1989; personal comml<strong>l1</strong>ication).<br />
Allen (1981: 141) has compared these points with nine similar ones<br />
excavated al the Rosenkrans site in New Jersey, a Middlesex Burial site. Kraft<br />
(1976: 32) proposes that these may have beer. the projectile point style used by<br />
people <strong>of</strong> the Middlesex cullure. However, these appear to resemble more<br />
closely Susquehanna Broad points, attributed to the Frost Island Phase 01 New<br />
York state (Ritchie 1969a: 158, Plale 51, Nos. 5·14, 18).<br />
The distribution <strong>of</strong> Group 3 ste<strong>l1</strong>'VTled bifaces matches thai <strong>of</strong> the<br />
Susquehanna Tracfrtion in the region. with roe notable exception. This is in<br />
northeastern New Brunswick, an area with a minimal mmber <strong>of</strong> recovered<br />
Susquehanna artifacts. As mentioned above. two possible Susquehanna<br />
artifacts were recovered from Red lJank and a potentially related burial exists on<br />
the southern sh<strong>of</strong>e <strong>of</strong> the S1. lawrence River; however. more research is<br />
necessary to ascertain a Susquehanna rxesence in this area.<br />
Chipping and grinding technology for the manufacture <strong>of</strong> celts also<br />
represents a Susquehanna Tradition trait present in the Early Ceramic Period.<br />
These forms. however, are not as densely distributed as Group 3 stemmed<br />
bifaces. Specimens are known from the Augustine and McKinlay siles (Turnbull<br />
1976. 1986) in New Brunswick and the Goddard site in Maine. At the latter site,<br />
two <strong>of</strong> these were associated with a radiocarbon dale <strong>of</strong> 2300±120 B.P.